Kenai Fjords National Park contains an impressive array of places that reflect the history, cultural richness, and changing relationship between people and the environment. These places encompass rugged glacially carved fjords, alpine mountainsides, the Harding Icefield, and braided river valleys.
What makes these places special? It is the varied uses and stories that we associate with them. Their significance may be worthy of a listing on our Nation's National Register of Historic Places, or they may significant to us on a personal level. Either way, there are amazing places to be preserved in Kenai Fjords.
The Exit Glacier area of Kenai Fjords National Park is the most publicly accessible part of park and the only portion that is accessible by road from the town of Seward. A number of individuals and families from the Seward area visit the Exit Glacier area in the course of recreational and resource harvesting activities within the park and the greater Resurrection River Valley.
Prior to the establishment of the park in 1980, this area was used for various activities including, hunting, guiding, berry picking, snow machining, horseback riding, snow shoeing, skiing, hiking, and gold mining. The importance of the area's resources played an important part in the quality of life experienced by nearby Seward residents.
A series of interviews were held in recent years with an exceptional group of men and women who used the Exit Glacier area prior to the establishment of Kenai Fjords National Park. While the activities they participated in may have been distinct, they all shared a common appreciation for the land and its resources. The wealth of their knowledge speaks to the kinds of joys and struggles experienced by today's visitors to the Exit Glacier area.
These interviews are accessible at Exit Glacier Project Jukebox.
To learn more about the project and what was learned from it, see A Study of Traditional Activities in the Exit Glacier Area of Kenai Fjords National Park.
Harding Ice Cap Camp - Kenai Fjords National Park Resource Brief, 2011
Nuka Bay is located on the outer, southwest coast of the Kenai Peninsula. No roads exist to the site and travel by boat and float plane are the primary means of transportation in and out of the bay. Sixty air miles southwest of Seward, and forty miles east of Homer, this area contains numerous sites of historic, ethnographic, and natural interest. The core historic sites are 1920-1940 mining sites typical of gold mining technology and techniques used in the mid-20th century. From a landscape perspective, the mining sites illustrate how the techniques of lode mining were adapted and applied to the extreme and challenging topography, vegetation and climate of the southern Kenai coast.
Stories abound of the riches to be had in the Nuka Bay District in the early 1900s. Seward's local paper, The Seward Gateway, regularly reported on the news brought up from the mining camps. While naysayers ridiculed the endeavors of the speculators and miners, the newspaper scoffed and supported the miners with articles touting the value of the Nuka Bay mines. It was even reported that the grass in Nuka grew tall as a result of the gold enriched the soils.
While the expectation of rich finds and gold bricks did not pan out as hoped, the Nuka Bay Mining District continues to be significant as a technological record of early 20th lode mining and a source of inspiration generated by the efforts of men and women who weren't afraid to work hard and dream big.
For more information on mining in the Nuka Bay Mining District, refer to the park's historic resource study, A Stern and Rockbound Coast.
History of the town of Seward - Seward Historic Preservation Commission
Red Light District Ethnohistory in Seward, Alaska By Rachel Mason
Did You Know?
“Killer whales” or orcas are actually quite friendly and often inquisitive about humans. In fact, the group of “resident killer whales” pictured here feeds entirely on fish. Only “transient killer whales” eat marine mammals. No wild killer whale has ever hurt a human being.